Artigo Revisado por pares

The westernmost sector of the lower-Cambrian Los Navalucillos Formation: microbialites in tidal deposits, Central Iberian Zone, Toledo Mountains, Spain

2019; Spanish National Research Council; Volume: 75; Issue: 2 Linguagem: Inglês

ISSN

1988-3250

Autores

Silvia Menéndez, Marta Rodríguez Martínez, Elena Moreno‐Eiris, Antonio Perejón,

Tópico(s)

Paleontology and Evolutionary Biology

Resumo

In the Central Iberian Zone of the Iberian Massif, the Los Navalucillos Formation, interpreted as tidal and shallow-marine carbonate deposits, contains a significant archaeocyathan faunal assemblage. Two new characteristic exposures are described here from the westernmost outcrops of the formation, close to La Nava de Ricomalillo area: (i) La Estrella, where the rocks are strongly affected by contact metamorphism due to the nearby plutonic complex; and (ii) the Finca Higueruela succession, without calcimicrobial-archaeocyathan boundstones, although different microbialites as stromatolites and oncolites are conspicuous.

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